End-Permian mass extinction in the oceans: an ancient analog for the twenty-first century?
JL Payne, ME Clapham - Annual Review of Earth and Planetary …, 2012 - annualreviews.org
The greatest loss of biodiversity in the history of animal life occurred at the end of the
Permian Period (∼ 252 million years ago). This biotic catastrophe coincided with an interval …
Permian Period (∼ 252 million years ago). This biotic catastrophe coincided with an interval …
Carbon-isotope stratigraphy across the Permian–Triassic boundary: a review
C Korte, HW Kozur - Journal of Asian Earth Sciences, 2010 - Elsevier
The Palaeozoic–Mesozoic transition is marked by distinct perturbations in the global carbon
cycle resulting in a prominent negative carbon-isotope excursion at the Permian–Triassic (P …
cycle resulting in a prominent negative carbon-isotope excursion at the Permian–Triassic (P …
Calibrating the end-Permian mass extinction
S Shen, JL Crowley, Y Wang, SA Bowring, DH Erwin… - science, 2011 - science.org
The end-Permian mass extinction was the most severe biodiversity crisis in Earth history. To
better constrain the timing, and ultimately the causes of this event, we collected a suite of …
better constrain the timing, and ultimately the causes of this event, we collected a suite of …
Multiple episodes of extensive marine anoxia linked to global warming and continental weathering following the latest Permian mass extinction
Explaining the~ 5-million-year delay in marine biotic recovery following the latest Permian
mass extinction, the largest biotic crisis of the Phanerozoic, is a fundamental challenge for …
mass extinction, the largest biotic crisis of the Phanerozoic, is a fundamental challenge for …
Rapid expansion of oceanic anoxia immediately before the end-Permian mass extinction
GA Brennecka, AD Herrmann… - Proceedings of the …, 2011 - National Acad Sciences
Periods of oceanic anoxia have had a major influence on the evolutionary history of Earth
and are often contemporaneous with mass extinction events. Changes in global (as …
and are often contemporaneous with mass extinction events. Changes in global (as …
Terrestrial–marine teleconnections in the collapse and rebuilding of Early Triassic marine ecosystems
The latest Permian mass extinction (LPE), just prior to the Permian–Triassic boundary at~
252Ma, resulted in the disappearance of~ 90% of skeletonized marine taxa and the …
252Ma, resulted in the disappearance of~ 90% of skeletonized marine taxa and the …
The end-Permian regression in South China and its implication on mass extinction
H Yin, H Jiang, W Xia, Q Feng, N Zhang, J Shen - Earth-Science Reviews, 2014 - Elsevier
Records of more than 20 Permian-Triassic Boundary (PTB) sections from South China show
that widespread end-Permian regression took place in whole South China. Timing of the low …
that widespread end-Permian regression took place in whole South China. Timing of the low …
[HTML][HTML] The stability and collapse of marine ecosystems during the Permian-Triassic mass extinction
The history of Earth's biodiversity is punctuated episodically by mass extinctions. These are
characterized by major declines of taxon richness, but the accompanying ecological …
characterized by major declines of taxon richness, but the accompanying ecological …
Calcium isotope constraints on the end-Permian mass extinction
The end-Permian mass extinction horizon is marked by an abrupt shift in style of carbonate
sedimentation and a negative excursion in the carbon isotope (δ 13C) composition of …
sedimentation and a negative excursion in the carbon isotope (δ 13C) composition of …
Microbialites and global environmental change across the Permian–Triassic boundary: a synthesis
Abstract Permian–Triassic boundary microbialites (PTBMs) are thin (0.05–15 m) carbonates
formed after the end‐Permian mass extinction. They comprise Renalcis‐group …
formed after the end‐Permian mass extinction. They comprise Renalcis‐group …